Studies on the topic of mathematical modeling of reservoir filtration and capacitance properties were carried out in the department for the creation and monitoring of geological models of the PermNIPIneft Branch of LUKOIL-Engineering LLC in Perm. The basis for the work was the need to test the method of the hydraulic flow unit at the Perm region deposit. The main task was to identify the regularities and characteristics of each class of the reservoir, separated by the indicator of the hydraulic flow unit. Graphical and geological-statistical processing of information was carried out using MS Excel, Statistica and IRAP RMS. For the study, a geological model of the Bb bed of the Moskudinskoye field was chosen.
For the facial complex of the delta channel, isolated during the core analysis and geophysical studies of the wells, some dependencies of the decrease in filtration-capacitive properties with depth increase were determined using the hydraulic flow unit indicator. Groups of values are defined that form linear equations with similar values of the angular coefficient. The features of each group are considered taking into account their getting into this or that class of the collector. A number of factors influencing the differences in changes in the properties of the reservoir were formed.
The most thoroughly investigated was the assumption of a clay material. Analyzing the graphs of the distribution of the coefficient of clayiness with depth for each of the isolated groups, the hypothesis was confirmed: with increasing depth, the coefficient of clayiness increases, thereby reducing the filtration-capacitive properties.
From the presented geological and statistical section of the previously identified groups, it became clear that the top of the section is represented to a greater degree by the rocks belonging to the group possessing the best filtration and capacitance properties. To the bottom of the section, the predominance of rocks of the group with lower properties is increasing.
The carried out researches allow to draw the following conclusion. The allocated groups have a different degree of accumulation of clay material. Greater clay is traced below the level of water-oil contact. The change in the properties of the clay material during the development of the deposits will worsen the reservoir filtration and capacitance properties. This decompaction, in turn, is the source of the energy of the reservoir for the selected groups. Differentiation of these groups makes it possible to specify in which sections of collectors these processes will pass, and in which they will not be significant. This will allow us to correctly understand the development of deposits, the design of drilling new wells and the adaptation of geological and hydrodynamic models